Mostrar el registro sencillo del ítem

dc.contributor.author Wolfensberger, Daniel
dc.contributor.author Scipión, Danny
dc.contributor.author Berne, Alexis
dc.date.accessioned 2018-07-24T14:21:21Z
dc.date.available 2018-07-24T14:21:21Z
dc.date.issued 2015-09-22
dc.identifier.govdoc index-oti2018 (NB)
dc.identifier.issn 1477-870X
dc.identifier.uri http://repositorio.igp.gob.pe/handle/IGP/2058
dc.description En: Quaterly Journal of the Royal Meteorological Society, v. 142, n. S1, (September 2015), p. 108-124. Este artículo también apareció en: Advances in understanding and forecasting of heavy precipitation in the Mediterranean through the HyMeX SOP1 field campaign. es_ES
dc.description.abstract "Stratiform rain situations are generally associated with the presence of a melting layer characterized by a strong signature in polarimetric radar variables. This layer is an important feature as it indicates the transition from solid to liquid precipitation. The melting layer remains poorly characterized, particularly from a polarimetric radar point of view. In this work a new algorithm to automatically detect the melting layer on polarimetric RHI radar scans using gradients of reflectivity and copolar correlation is first proposed. The algorithm was applied to Xband polarimetric radar data and validated by comparing the height of the detected layer with freezing levels heights obtained from radiosoundings and was shown to give both small errors and bias. The algorithm was then used on a large selection of precipitation events (more than 4000 RHI scans) from different seasons and climatic regions (South of France, Swiss Alps and plateau and Iowa-USA) to characterize the geometric and polarimetric signatures of the melting layer. The melting layer is shown to have a very similar geometry on average, independently of the topography and climatic conditions. Variations in the thickness of the melting layer during and between precipitation events was shown to be strongly related to the presence of rimed particles, to the vertical velocity of hydrometeors and to the intensity of the bright band." es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher Instituto Geofísico del Perú es_ES
dc.rights info:eu-repo/semantics/restrictedAccess es_ES
dc.rights.uri info:eu-repo/semantics/restrictedAccess es_ES
dc.source Repositorio institucional - IGP es_ES
dc.subject Polarimetría es_ES
dc.subject Reflectancia es_ES
dc.subject Lluvia y precipitación es_ES
dc.subject Climatología es_ES
dc.subject Correlación estratigráfica es_ES
dc.title Detection and characterization of the melting layer based on polarimetric radar scans es_ES
dc.type info:eu-repo/semantics/article es_ES
dc.subject.ocde Precipitación es_ES
dc.subject.ocde Radar es_ES
dc.subject.ocde Teledetección polarimétrica es_ES
dc.subject.ocde Clima es_ES
dc.subject.ocde Topografía es_ES
dc.identifier.journal Quarterly Journal of the Royal Meteorological Society es_ES
dc.description.peer-review Por pares es_ES
dc.identifier.doi 10.1002/qj.2672 es_ES

Thumbnail

 Bloqueado

Colecciones

Mostrar el registro sencillo del ítem